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Results:

• 11. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 12. Traffc-maintenance_expenditures

  047 13 903 11 197 - - - 522 610 1 406 449 1980 42 409 153 761 14 024 212 220 - 5 257 17 816 10 410 9 234 - - - 465 133 1 420 546 Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land /media/loftslag/Traffc-maintenance_expenditures.pdf

• 13. VI_2015_006

  ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 14. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 15. vanRoosmalen_etal-2009-WRR_2007WR006760

  is completely saturated and the unsaturated zone no longer active. The net horizontal boundary outflow is the Figure 5. Observed and simulated groundwater heads at locations A and B in Figure 2. W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE 9 of 18 W00A15 net outflow across the catchment boundary and accounts primarily for groundwater flow to the sea. Drain flow includes drainage from groundwater /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 16. GA_2009_91A_4_Andreassen

  and asimplified mass balance model suggests that airtemperature and albedo is satisfactorily parameter-ised, at least for the AWS altitude. However, thecompared period covers only 5 of the 58 modelledyears in this study. Furthermore, the specific win-ter, summer and net balances measured at Stor-breen in 2001–2006 deviate markedly from the mean for the whole observation period. A combi-nation /media/ces/GA_2009_91A_4_Andreassen.pdf

• 17. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 18. Joining forces in weather forecasting and climate research

  Snorrason, Director General of the IMO. The new supercomputer can perform 4,000 trillion calculations per second, which is more than half a million calculations per second for every person on the planet. It will handle state of the art weather models with more than 6 million lines of code –the Mars Curiosity Rover was built on 5 million- which will produce high resolution weather predictions /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 19. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 20. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf